Provenancing Archaeological Wool Textiles from Medieval Northern Europe by Light Stable Isotope Analysis (δ13C, δ15N, δ2H)

We investigate the origin of archaeological wool textiles preserved by anoxic waterlogging from seven medieval archaeological deposits in north-western Europe (c. 700-1600 AD), using geospatial patterning in carbon (δ13C), nitrogen (δ15N) and non-exchangeable hydrogen (δ2H) composition of modern and ancient sheep proteins. δ13C, δ15N and δ2H values from archaeological wool keratin (n = 83) and bone collagen (n = 59) from four sites were interpreted with reference to the composition of modern sheep wool from the same regions. The isotopic composition of wool and bone collagen samples clustered strongly by settlement; inter-regional relationships were largely parallel in modern and ancient samples, though landscape change was also significant. Degradation in archaeological wool samples, examined by elemental and amino acid composition, was greater in samples from Iceland (Reykholt) than in samples from north-east England (York, Newcastle) or northern Germany (Hessens). A nominal assignment approach was used to classify textiles into local/non-local at each site, based on maximal estimates of isotopic variability in modern sheep wool. Light element stable isotope analysis provided new insights into the origins of wool textiles, and demonstrates that isotopic provenancing of keratin preserved in anoxic waterlogged contexts is feasible. We also demonstrate the utility of δ2H analysis to understand the location of origin of archaeological protein samples

Ochratoxin A in Portugal: A Review to Assess Human Exposure

In Portugal, the climate, dietary habits, and food contamination levels present the characteristics for higher population susceptibility to ochratoxin A (OTA), one of the known mycotoxins with the greatest public health and agro-economic importance. In this review, following a brief historical insight on OTA research, a summary of the available data on OTA occurrence in food (cereals, bread, wine, meat) and biological fluids (blood, urine) is made. With this data, an estimation of intake is made to ascertain and update the risk exposure estimation of the Portuguese population, in comparison to previous studies and other populations

Key drivers controlling stable isotope variations in daily precipitation of Costa Rica: Caribbean Sea versus Eastern Pacific Ocean moisture

2013-2017: International Atomic Energy Agency, Vienna, Austria, Project CRP 17947: Stable isotopes in precipitation and paleoclimatic archives in tropical areas to improve regional hydrological and climatic impact modelsCosta Rica is located on the Central American Isthmus, which receives moisture inputs directly from the Caribbean Sea and the Eastern Pacific Ocean. This location includes unique mountainous and lowland microclimates, but only limited knowledge exists about the impact of relief and regional atmospheric circulation patterns on precipitation origin, transport, and isotopic composition. Therefore, the main scope of this project is to identify the key drivers controlling stable isotope variations in daily-scale precipitation of Costa Rica. The monitoring sites comprise three strategic locations across Costa Rica: Heredia (Central Valley), Turrialba (Caribbean slope), and Caño Seco (South Pacific slope). Sporadic dry season rain is mostly related to isolated enriched events ranging from −5.8‰ to −0.9‰ δ18O. By mid-May, the Intertropical Convergence Zone reaches Costa Rica resulting in a notable depletion in isotope ratios (up to −18.5‰ δ18O). HYSPLIT air mass back trajectories indicate the strong influence on the origin and transport of precipitation of three main moisture transport mechanisms, the Caribbean Low Level Jet, the Colombian Low Level Jet, and localized convection events. Multiple linear regression models constructed based on Random Forests of surface meteorological information and atmospheric sounding profiles suggest that lifted condensation level and surface relative humidity are the main factors controlling isotopic variations. These findings diverge from the recognized ‘amount effect’ in monthly composite samples across the tropics. Understanding of stable isotope dynamics in tropical precipitation can be used to a) enhance groundwater modeling efforts in ungauged basins where scarcity of long-term monitoring data drastically limit current and future water resources management, b) improve the re-construction of paleoclimatic records in the Central American land bridge, c) calibrate and validate regional circulation models.Costa Rica está ubicada en el Istmo Centroamericano, que recibe aportes de humedad directamente del Mar Caribe y del Océano Pacífico Oriental. Esta ubicación incluye microclimas montañosos y de tierras bajas únicas, pero solo existe un conocimiento limitado sobre el impacto del relieve y los patrones de circulación atmosférica regional sobre el origen, el transporte y la composición isotópica de las precipitaciones. Por lo tanto, el alcance principal de este proyecto es identificar los impulsores clave que controlan las variaciones de isótopos estables en la precipitación a escala diaria de Costa Rica. Los sitios de monitoreo comprenden tres ubicaciones estratégicas en Costa Rica: Heredia (Valle Central), Turrialba (vertiente del Caribe) y Caño Seco (vertiente del Pacífico Sur). La lluvia esporádica de la estación seca se relaciona principalmente con eventos enriquecidos aislados que van desde −5,8 ‰ a −0,9 ‰ δ18O. A mediados de mayo, la Zona de Convergencia Intertropical llega a Costa Rica, lo que resulta en un notable agotamiento de las proporciones de isótopos (hasta −18,5 ‰ δ18O). Las trayectorias de retroceso de la masa de aire de HYSPLIT indican la fuerte influencia en el origen y transporte de la precipitación de tres mecanismos principales de transporte de humedad, el chorro de bajo nivel del Caribe, el chorro de bajo nivel de Colombia y los eventos de convección localizados. Múltiples modelos de regresión lineal construidos a partir de bosques aleatorios de información meteorológica de superficie y perfiles de sondeo atmosférico sugieren que el nivel de condensación elevado y la humedad relativa de la superficie son los principales factores que controlan las variaciones isotópicas. Estos hallazgos difieren del "efecto de cantidad" reconocido en muestras compuestas mensuales en los trópicos. La comprensión de la dinámica de isótopos estables en la precipitación tropical se puede utilizar para a) mejorar los esfuerzos de modelado de aguas subterráneas en cuencas no calibradas donde la escasez de datos de monitoreo a largo plazo limita drásticamente la gestión actual y futura de los recursos hídricos, Puente terrestre centroamericano, c) calibrar y validar modelos de circulación regional.Escuela de Químic

Accelerated thermal profiling of gas turbine components using luminescent thermal history paints

Environmental requirements to reduce CO2 emissions and the drive towards higher efficiencies have resulted in increased operating temperatures in gas turbines. Subsequently, Original Equipment Manufacturer (OEMs) require improved component design and material selection to withstand the harsher conditions. This demands rapid evaluation of new components and their surface temperature to accelerate their market entry. Accurate temperature information proves key in the design of more efficient, longer-lasting machinery and in monitoring thermal damage. A number of traditional temperature measurement techniques are available, but can incur a number of limitations. Online temperature measurements, such as pyrometry or phosphor thermography, often require optical access to the component during operation and are therefore not suitable for inaccessible components. Other options including thermocouples can only provide point measurements and cannot deliver profiles across the surface. Offline techniques store temperature information that can be measured and analysed following operation. Several of these, however, are of destructive nature, can affect local thermal gradients and only provide point measurements. This article discusses an innovative offline measurement technique: luminescent Thermal History Paints (THPs). THPs are comprised of ceramic pigments in a binder matrix that can be applied to any hot component as a thin coating. These pigments are doped with optically active ions, which will phosphoresce when excited with a light source. The coating material experiences irreversible structural changes depending on the temperature it is exposed to. Changes in the material structure are reflected in its phosphorescent properties, which are measured with standard optical instrumentation at any surface location. Since the changes are permanent, the temperature information is stored in the coating and can be extracted after operation. Following calibration, it is therefore possible to relate phosphorescent behaviour to the past maximum temperature experienced at each location. This is done with Sensor Coating Systems Ltd. (SCS)’s portable instrumentation, which can provide rapid, automated and objective measurements across a component surface. Unlike the more traditional thermal paints, THPs are non-toxic, and provide a continuous measurement capability across the range 150°C–900°C with significantly improved durability. This article describes the underlying principles behind this novel technology and the advantages it provides over existing state-of-the-art methods. The benefits will be demonstrated through measurements on nozzle guide vanes (NGVs), with the view to compare and validate them against thermocouple measurements. The results show that the THP extends the limited information from thermocouples to provide a more complete view of the thermal processes on the component